Inferring surface water equilibrium calcite δ 18 O during the last deglacial period from benthic foraminiferal records: Implications for ocean circulation-Reference-Cited by-同舟云学术

Inferring surface water equilibrium calcite δ 18 O during the last deglacial period from benthic foraminiferal records: Implications for ocean circulation

Published:2015-11 Issue:11 Volume:30 Page:1470-1489
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Amrhein Daniel E.¹^ORCID,Gebbie Geoffrey²,Marchal Olivier²,Wunsch Carl³

Affiliation:

1. Massachusetts Institute of Technology‐Woods Hole Oceanographic Institution Joint Program in Oceanography Cambridge Massachusetts USA

2. Woods Hole Oceanographic Institution Woods Hole Massachusetts USA

3. Department of Earth and Planetary SciencesHarvard University Cambridge Massachusetts USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2014PA002743

Reference77 articles.

1. The Salinity, Temperature, and δ 18 O of the Glacial Deep Ocean

2. Amrhein D. E.(2014) An inverse approach to understanding deglacial benthic oxygen isotope records Master's thesis Mass. Inst. of Technol. / Woods Hole Oceanogr. Inst. Cambridge.

3. Retreat velocity of the North Atlantic polar front during the last deglaciation determined by 14C accelerator mass spectrometry

4. Interhemispheric Atlantic seesaw response during the last deglaciation

5. A multiproxy reconstruction of the evolution of deep and surface waters in the subarctic Nordic seas over the last 30,000yr

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